Method for determination of real subsoil geological formation

ABSTRACT

The present disclosure relates to a method for determination of a real subsoil geological formation. In at least one embodiment, the method includes receiving a model representing the real subsoil. The model includes a stratigraphic layer, and the stratigraphic layer includes a shore line dividing the stratigraphic layer into a continental zone and a marine zone. The method further includes receiving a first flow speed field representative of a continental domain for the stratigraphic layer, and receiving a second flow speed field representative of a marine domain for the stratigraphic layer. A global flow speed field is determined and includes a weighted combination of the first flow speed field and the second flow speed field for each position in the stratigraphic layer, and weights of the combination are based on a distance of said position to the shore line and the fact that the position is within the continental zone or the marine zone. The method further includes determining a real subsoil geological formation for the stratigraphic layer based on the determined global flow speed field.

BACKGROUND OF THE DISCLOSURE

The present disclosure relates to determination of subsoil formations,especially for the use in the hydrocarbon industries.

The approaches described in this section could be pursued, but are notnecessarily approaches that have been previously conceived or pursued.Therefore, unless otherwise indicated herein, the approaches describedin this section are not prior art to the claims in this application andare not admitted to be prior art by inclusion in this section.Furthermore, all embodiments are not necessarily intended to solve allor even any of the problems brought forward in this section.

In the past, when a subsoil formation should be determined, a sameparadigm is used: “the model used for said determination should bemeshed before any modeling”.

Indeed, for any modeling methods, the meshing is mandatory.

Nevertheless, it is well known that this meshing prior to any modelinghas several drawbacks as the size of the meshes, the orientation of themeshes, and the number of the meshes that induce a bias in the modeling.

For instance, this meshing prior to any modeling cannot take intoaccount the sedimentary bodies/formations of the subsoil which will beidentified during the modeling phase.

It is noted that the accurate determination of the subsoilstructures/formations is a key feature for determining hydrocarbonreservoirs and enabling a proper industrial production plan/productionof hydrocarbons.

In addition, when working with pre-meshed models, it may be difficult toaccurately satisfy at the well constraints (i.e. log data) as with thelog data where it must be transformed with blocking methods to adapt theprecision of the log data to the dimension of the cells.

It is also noted that in the prior art, when geological objects aremodeled, the main constraint used is the probability of occurrences ofsaid objects in a given zone. In particular, the specific relation(s)between the object of the zones are not taken into account (forinstance, some objects may only exist in connection to/closeto/downstream to other specific object(s)).

Furthermore, in prior art methods, it may be difficult to associate thecells with facies or geophysical property as the dimension of the celldoes not allow a proper identification of their respective position inthe geological formations.

SUMMARY OF THE DISCLOSURE

The disclosure relates to a method for determination of real subsoilformation characterized in that the method comprises:

-   -   /a/ receiving a model representing the real subsoil, said model        comprising a stratigraphic layer, said stratigraphic layer        comprising a shore line dividing the stratigraphic layer into a        continental zone and a marine zone;    -   /b/ receiving a first flow speed field for the stratigraphic        layer;    -   /c/ receiving a second flow speed field representative of a sea        for the stratigraphic layer;    -   /d/ determining a weighted combination, named global flow speed        field, of the first flow speed field and the second flow speed        field for each position in the stratigraphic layer, weights of        the combination are based on a distance of said position to the        shore line and the fact that the position is within the        continental zone or the marine zone    -   /e/ determining a real subsoil geological formation for the        stratigraphic layer based on the determined global flow speed        field.

The received second flow speed field may be determined based onhydrodynamic modeling.

The received second flow speed field may be determined based on theshore line.

Before the computation of the global flow speed field, the first flowspeed may be modified to align a gradient of the first flow speed fieldwith the shore line.

The model may comprise a plurality of stratigraphic layers, eachstratigraphic layer within said plurality may comprise a respectiveshore line dividing the stratigraphic layer into a respectivecontinental zone and a respective marine zone.

Steps /b/ to /e/ may be reiterated for each stratigraphic layer withinsaid plurality.

The respective shore line for each stratigraphic layer within saidplurality may be different from the respective shore line for the otherstratigraphic layer within said plurality.

An intersection between the transitional zone and the continental zonemay be void or may be the shore line.

The disclosure is also directed to a device for determination of realsubsoil geological formation characterized in that the device comprises:

-   -   /a/ an interface for receiving a model representing the real        subsoil, said model comprising a stratigraphic layer, said        stratigraphic layer comprising a shore line (800) dividing the        stratigraphic layer into a continental zone (801) and a marine        zone (802);    -   /b/ an interface for receiving a first flow speed field (811)        for the stratigraphic layer;    -   /c/ an interface for receiving a second flow speed field (812)        representative of a sea for the stratigraphic layer;    -   /d/ a circuit for determining a weighted combination, named        global flow speed field, of the first flow speed field and the        second flow speed field for each position in the stratigraphic        layer, weights of the combination are based on a distance of        said position to the shore line (800) and the fact that the        position is within the continental zone or the marine zone    -   /e/ a circuit for determining the real subsoil composition for        the stratigraphic layer based on the determined global flow        speed field.

The disclosure is also directed to a non-transitory computer readablestorage medium, having stored thereon a computer program comprisingprogram instructions, the computer program being loadable into adata-processing unit and adapted to cause the data-processing unit tocarry out the steps of the method described above when the computerprogram is run by the data-processing device.

The disclosure is also directed to a method for determination of realsubsoil geological formation characterized in that the method comprises:

-   -   /a/ receiving a model representing the real subsoil,    -   /b/ determining a first fluvial geological formation in said        model using parametric surfaces,    -   /c/ determining a subsequent fluvial geological formation as a        deformation of the first fluvial geological formation using        parametric surfaces,    -   /d/ subtract the first fluvial geological formation from the        subsequent fluvial geological formation to create a new        geological formation named point bar formation.

The determining of a first fluvial geological formation may be performedbased on a stochastic process.

The deformation of step /c/ may comprise:

-   -   determining inflection points of a trajectory of the first        fluvial formation, said trajectory being in the parametric        surface of the first fluvial formation;    -   modifying the trajectory of the first fluvial formation to        create a trajectory of the subsequent fluvial formation, said        trajectory of the subsequent fluvial formation passing through        the inflection points;    -   defining parametric surface of the subsequent fluvial formation        based on the trajectory of the subsequent fluvial formation.

Steps /c/ to /d/ may be reiterated to create a plurality of point barformations.

A respective flow transmissivity parameter may be associated with eachone of the plurality of point bar formations, the respective flowtransmissivity parameter for a given point bar formation determinedduring the iteration n being greater than the respective flowtransmissivity parameter for a given point bar formation determinedduring the iteration n+1.

Therefore; it is possible to compute a fluid flow simulation based onsaid transmissivity parameter.

The disclosure is also directed to a device for determination of realsubsoil geological formation characterized in that the device comprises:

-   -   /a/ an interface for receiving a model representing the real        subsoil,    -   /b/ a circuit for determining a first fluvial geological        formation in said model using parametric surfaces,    -   /c/ a circuit for determining a subsequent fluvial geological        formation as a deformation of the first fluvial geological        formation using parametric surfaces,    -   /d/ a circuit for subtract the first fluvial geological        formation from the subsequent fluvial geological formation to        create a new geological formation named point bar formation.    -   /e/ a circuit for determine a real subsoil composition for the        point bar formation.

The disclosure is also directed to a non-transitory computer readablestorage medium, having stored thereon a computer program comprisingprogram instructions, the computer program being loadable into adata-processing unit and adapted to cause the data-processing unit tocarry out the steps of the method described above when the computerprogram is run by the data-processing device.

The disclosure is also directed to a method for determination of realsubsoil geological formation characterized in that the method comprises:

-   -   /a/ receiving a model representing the real subsoil,    -   /b/ determine a first stochastic trajectory of a first fluvial        formation in said model,    -   /c/ defining a constraint zone comprising said first fluvial        formation,    -   /d/ determining a second stochastic trajectory of a second        fluvial formation in said model within said constraint zone        based on a stochastic process.

Edges of the constraint zone may be within a predetermined distance tothe first stochastic trajectory of a first fluvial formation.

Step /d/ may be reiterated a predetermined number of time.

Steps /c/ to step /d/ may be reiterated, in said reiteration, the secondfluvial formation may be taken as the first fluvial formation and athird stochastic trajectory of a third fluvial formation may be taken asa second stochastic trajectory of a second fluvial formation.

Step /d/ may comprise a displacement of the constraint zone according toa given direction between iterations

Determining the second stochastic trajectory may comprise:

-   -   /d1/ determining a point of the model based on the stochastic        process,    -   /d2/ if said point is outside the constraint zone, reiterating        steps /d1/ and /d2/ , otherwise, adding said point to the second        stochastic trajectory wherein if the reiteration of steps /d1/        and /d2/ exceeds a predetermined number, the determining of        second stochastic trajectory is reinitialized.

Determining the second stochastic trajectory may comprise:

-   -   /d1/ determining a point of the second stochastic trajectory,    -   /d2/ if said point is outside the constraint zone, changing        coordinates of said point to a closest point of the constraint        zone.

Determining the second stochastic trajectory may comprise:

-   -   /d1/ determining a point of the second stochastic trajectory,    -   /d2/ if said point is outside the constraint zone, reiterating        steps /d1/ and /d2/

wherein if the reiteration of steps /d1/ and /d2/ exceeds apredetermined number, coordinates of said point is changed to a closestpoint of the constraint zone.

The disclosure is also directed to a device for determination of realsubsoil geological formation characterized in that the device comprises:

-   -   /a/ an interface for receiving a model representing the real        subsoil,    -   /b/ a circuit for determining a first stochastic trajectory of a        first fluvial formation in said model,    -   /c/ a circuit for defining a constraint zone comprising said        first fluvial formation,    -   /d/ a circuit for determining a second stochastic trajectory of        a second fluvial formation in said model within said constraint        zone based on a stochastic process.

The disclosure is also directed to a non-transitory computer readablestorage medium, having stored thereon a computer program comprisingprogram instructions, the computer program being loadable into adata-processing unit and adapted to cause the data-processing unit tocarry out the steps of the method described above when the computerprogram is run by the data-processing device.

The disclosure is also directed to a method for determination of realsubsoil geological formation characterized in that the method comprises:

-   -   /a/ receiving a model representing the real subsoil, said model        comprising a shore line (1000) and a fluvial formation (1003)        connected to said shore line at a point (1006) of the model,        said shore line dividing the model into a marine zone and a        continental zone,    -   /b/ determining a delta zone in the model based on the shore        line and based on the fluvial formation,    -   /c/ determining a stochastic trajectory in said delta zone,    -   /d/ determining a lobe formation in said delta zone based on the        determined stochastic trajectory based on a stochastic process.

The determined delta zone may be parametrized by a delta angle and adelta length.

The delta angle and the delta length may be determined based on a flowspeed in the fluvial formation.

The delta angle and the delta length may be determined based on a flowspeed in the marine zone.

It is also possible to determine a tidal bar formation along thestochastic trajectory.

The disclosure is also directed to a device for determination of realsubsoil geological formation characterized in that the device comprises:

-   -   /a/ an interface for receiving a model representing the real        subsoil, said model comprising a shore line (1000) and a fluvial        formation (1003) connected to said shore line at a point (1006)        of the model, said shore line dividing the model into a marine        zone and a continental zone,    -   /b/ a circuit for determining a delta zone in the model based on        the shore line and based on the fluvial formation,    -   /c/ a circuit for determining a stochastic trajectory in said        delta zone,    -   /d/ a circuit for determining a lobe formation in said delta        zone based on the determined stochastic trajectory based on a        stochastic process.

The disclosure is also directed to a non-transitory computer readablestorage medium, having stored thereon a computer program comprisingprogram instructions, the computer program being loadable into adata-processing unit and adapted to cause the data-processing unit tocarry out the steps of the method described above when the computerprogram is run by the data-processing device.

The disclosure is also directed to a method for determination of realsubsoil geological formation characterized in that the method comprises:

-   -   /a/ receiving a model representing the real subsoil,    -   /b/ receiving a proportions cube describing geological        properties of the model;    -   /c/ determining a permeability value for a plurality of        locations of the model based on the received proportions cube;    -   /d/ determining a gradient of the flow speed based on the        permeability value determined for a plurality of locations of        the model;    -   /e/ determining a fluvial formation based on the gradient of the        flow speed.

Based on the proportions cube, it is possible to determine apseudo-permeability value but to use it as a permeability value to solvethe fluid flow equations. Therefore, this is the reason that it iscorrect to determine a “permeability value” based on the“pseudo-permeability value”.

The determination of the gradient may comprise a solving of aDarcy-Weisbach equation.

The proportions cube may be a facies proportions cube,

The determination of the pseudo-permeability value may comprise a meanof respective permeability value of facies weighted by the proportion ofsaid facies according to the facies proportions cube.

Step /d/ comprises interpolation of the pseudo-permeability value forlocations of the model where no proportions cube is available.

The model may comprise a no-flow zone,

The pseudo-permeability value for location in said no-flow zone may beset to 0.

The disclosure is also directed to a device for determination of realsubsoil geological formation characterized in that the device comprises:

-   -   /a/ an interface for receiving a model representing the real        subsoil,    -   /b/ an interface for receiving a proportions cube describing        geological properties of the model;    -   /c/ a circuit for determining a pseudo-permeability value for a        plurality of locations of the model based on the received        proportions cube;    -   /d/ a circuit for determining a gradient of the flow speed based        on the pseudo-permeability value determined for a plurality of        locations of the model;    -   /e/ a circuit for determining a fluvial formation based on the        gradient of the flow speed.

The disclosure is also directed to a non-transitory computer readablestorage medium, having stored thereon a computer program comprisingprogram instructions, the computer program being loadable into adata-processing unit and adapted to cause the data-processing unit tocarry out the steps of the method described above when the computerprogram is run by the data-processing device.

Other features and advantages of the method and apparatus disclosedherein will become apparent from the following description ofnon-limiting embodiments, with reference to the appended drawings.

BRIEF DESCRIPTION OF THE DRAWINGS

The present disclosure is illustrated by way of example, and not by wayof limitations, in the figures of the accompanying drawings, in whichlike reference numerals refer to similar elements and in which:

FIG. 1 is a general workflow of a possible embodiment of the disclosure;

FIGS. 2a and 2b are respectively a 3D view of a fluvial geologicalformation and a top view of a fluvial geological formation;

FIG. 3a is a representation of surfaces/sides determination of a fluvialgeological formation with NURBS surfaces;

FIGS. 3b and 3c are 3D view of interconnected fluvial geologicalformations;

FIG. 4a is a top view of a distortion of a representation of ageological formation to satisfy a well constraint (horizontaldistortion);

FIG. 4b is a representation of well data and provides indication ondistortion of a geological formation to satisfy a well constraint(vertical distortion);

FIG. 5 provides examples regarding the meshing of geological formations;

FIGS. 6a and 6b are respectively a top view of associated geologicalformations and 3D view of said associated geological formations;

FIG. 6c provides examples regarding the meshing of associated geologicalformations;

FIG. 7a exemplifies a possible process for associating a facies to acell of a geological formation;

FIG. 7b exemplifies a possible process for associating a property to acell of a geological formation;

FIG. 8 is a possible embodiment for dynamically determining flow speedfield in the model/in the zone;

FIG. 9a is a possible embodiment for creating point bar zones such asdescribed in FIG. 6a, 6b or 6 c;

FIG. 9b is a possible embodiment for determining fluvial formations fordifferent stratigraphic layers;

FIG. 10 is a representation of the modeling of lobes (i.e. at an end ofthe fluvial formation) in marine zones of the model, especially in caseof tide-dominated deltas;

FIG. 11 is a representation of the modeling of the flow speed (or thegradient of the flow speed) in the model for a stratigraphic layer;

FIG. 12 is a possible embodiment for a device that enables oneembodiment (at least) of the present disclosure.

DETAILED DESCRIPTION

In the following description, fluvial geological formations aredescribed exemplifying the disclosure but it applies to any possiblegeological formations (e.g. lobes, turbiditic systems, etc.)

Therefore, in the following, “fluvial trajectory” may be replaced by“sediment trajectory” or “flow trajectory” without significantmodification.

FIG. 1 is a chart describing a possible process of the disclosure.

In this chart, the manipulated model is possibly a parametric model ofthe subsoil. A parametric model M_(p)(u,v,t) of the subsoil is atransformation of a 3D model M(x,y,z) of the subsoil.

A 3D model M(x,y,z) of a real subsoil describes the subsoil according toits real geographical coordinates (x,y,z) (i.e. at the present time).

A parametric model M_(p)(u,v,t) of said subsoil describes the state ofthe subsoil at a geological time t: each layer represents the state ofthe subsoil at the time t where the sedimentation occurs. One may saythat the parametric model M_(p)(u,v,t) restores the horizontal layer fora given sedimentation/geological time t.

In the manipulated model, it is possible to simulate the geologicalformation of a fluvial zone. Said geological formation determination ofa fluvial zone may comprise, as described in WO 2012/072923, thedisplacement of particles (step 101) in the manipulated model bysuperimposing:

-   -   a deterministic term defined on the basis of observation data        for the fluvial zone to be determined, and    -   a stochastic term parametrized at least by the observation data.

It is possible to take into account both the sedimentary flow in thezone, and to introduce a probabilistic perturbation.

When one speaks of superposition of two terms, it will be understoodthat the simulated displacement is composed from the sum of thedeterministic term and of the stochastic term.

The stochastic term can comprise the superposition of a meandriform termand of a random perturbation. So doing, the modeling of the channel isrendered more realistic.

The meandriform term can comprise a superposition of at least onetrigonometric function. Such a representation is realistic for ameandriform term, and easily parametrizable.

The observation data can comprise at least one of the following types ofdata:

-   -   a gradient of flow speed in the zone,    -   geometric parameters of the zone,    -   data arising from drilling,    -   data arising from imaging, especially seismic imaging.

It is noted that the model does not need to be meshed up to this point.A parametric description of the trajectory may be easily determined inthe model.

Once the respective trajectory 201 (see FIGS. 2a, 2b ) of geologicalformation(s) of a fluvial zone is/are determined (for the sake of theunderstanding, the singular is used in the following, considering thatonly one trajectory 201 is determined, but it is apparent that theplural may also be used), it is possible to determine surface(s) (step102) that represent the extend of the determined geological formation,the trajectory being inside said extends. This extends may represent thebed of a river/torrent/etc. or any geological formation of the fluvialzone (see element 202, FIGS. 2a, 2b ).

To describe these surfaces, it is possible to use NURBS (or Non-UniformRational B-Splines). Alternatively, in the followings, the use of NURBSsurfaces/lines may be any parametric surfaces/lines.

NURBS is a mathematical model used in computer graphics for generatingand representing curves and surfaces. It offers great flexibility andprecision for handling both analytic (surfaces defined by commonmathematical formulae) and modeled shapes.

Therefore there is no need to identify the bed of said formations byidentifying the meshes/cells of the meshed model that are inside thebed: a parametric description of said formations enables a far bettermeshing performed at a later stage fitting the NURBS surfaces.

For instance, in FIG. 3a , a side view of the model is shown, thetrajectory 201 being perpendicular to said view. In said figure,trajectory 201 is represented as a single point. When referring to“point 201”, one means the point corresponding to the intersectionbetween the view plan of figure and the trajectory 201.

To represent the extend of the determined geological formation, it ispossible to represent the shape of bed by a plurality of NURBS 310, 311and 312, ensuring that the contacts of these NURBS satisfy someparametric continuity (for instance C⁰, C¹ and/or C²) and/or somegeometric continuity (for instance G⁰, G¹ and/or G²).

In the example of FIG. 3a , point 303 and 309 may be defined such that303, 201 and 309 are aligned, the respective distance between 303-201and 201-309 may be function of the local curvature of the trajectory 201(see FIG. 2b ).

In said example, point 303 represents a point on the convex side of thecurvature of the trajectory 201; point 309 represents a point on theconcave side of the curvature of the trajectory 201. Thus, it ispossible to compute the distances 303-201 and 201-309 as a function ofthe local curvature of the trajectory 201 and such that the distance303-201 is lower than distance 309-201.

Point 306 may be determined such that the line (306;201) isperpendicular to the line (303;309) and such that the distance 306-201is either a predetermined value or function of the local curvature orfunction of the distance 303-309.

In addition, once the positions of points 306, 303 and 309 aredetermined, it is possible to determine a plurality of set of points304, 305, 307 and 308. These points may have a location function of thepositions of points 306, 303 and 309 and/or the curvature of trajectory201.

Points 303, 304, 305, 306 may define a first NURBS 311.

Points 309, 308, 307, 306 may define a second NURBS 310.

A third NURBS 312 may be defined to close the shape of the bed.

NURBS curves may be determined thanks to the Cox-de Boor's Algorithm.

This process is described in regard of a side view of the trajectory(perpendicular to said trajectory) but can be reiterated for a pluralityof different side views of the trajectory (see FIG. 2b for instance).Then, NURBS surfaces may be defined thanks to the NURBS curves (orthanks to points that have been used to define the NURBS curves).

The use of the NURBS surfaces is very effective as it is possible to“subtract” volumes of determined geological formations. For instance,referring to FIG. 3b , if two geological formations 320 and 321 aredetermined and if their respective volumes intersect each other,available NURBS Intersection algorithms (see for instance Patrikalakis,N. M., & Maekawa, T. (2010). Intersection problems. In ShapeInterrogation for Computer Aided Design and Manufacturing (pp. 109-160).Springer, Berlin, Heidelberg or Rossignac, J. R., & Requicha, A. A.(1987). Piecewise-circular curves for geometric modeling. IBM Journal ofResearch and Development, 31(3), 296-313) provide accurate and effectivemethod to subtract the volume of formation 321 to formation 320(representing the replacement of the formation 320 by formation 321 dueto hydrodynamic/fluvial erosion) to create the new volume 322 (FIG. 3c). Algorithms based on cells/meshes (i.e. identifying cells that are inboth formations) are not as accurate and effective as the NURBSalgorithms.

In addition, if the model has some constraints (e.g. a seismic orgeological indication that a formation is present at a given location),it is possible to distort the closest NURBS 320 to ensure that thisconstraint 401 (see FIG. 4a , which is a top view of the model) issatisfied. The distortion methods for NURBS surfaces are well available(for instance, Piegl, L., & Tiller, W. (2012). The NURBS book. SpringerScience & Business Media, chapter 11). Therefore it is possible tosatisfy all constraints of the model.

It is also possible to distort the formation vertically to match theconstraints but within a given distance/zone. For instance, if one maywant to satisfy the well-data (see FIG. 4b ) represented by layer411-416, it is possible to use the logs directly without applying ablocking method (which was mandatory in the method of the prior art,i.e. the reduction to coarser layers 421-423). Thanks to said method, ifit is known that a fluvial formation is in the layer 413 and that theclosest formation in the model is at position 430, it is easy to distortthe NURBS to satisfy the constraints. With a blocking method, thisconstraint may not be satisfied as the layer 413 may disappear.

Once the formations are determined thanks to the NURBS surfaces, it ispossible to mesh the formations (step 103 of FIG. 1) according to theformations surfaces definition.

A plurality of meshing is possible as described in FIG. 5. For instance,meshes 501, 502, 503 or 504 are possible. Well-known methods such as theQuadtree meshing method, the Octree meshing method, Front method,Delaunay method, Prograding grid, divergent grid, aggrading grid, etc.are usable.

It is possible to understand that the meshing performed a posteriori(i.e. after the determination of the formation shapes) is far better(i.e. fits the shape of the geological bodies) than a meshing performeda priori (i.e. before any shape determination of geological formation).

In addition, based on the first geological formations determined, it ispossible to create related formations such as lobes (i.e. at an end ofthe fluvial formation), bar, point bar (see FIGS. 6a and 6b , the numberof internal surfaces 601 or the distance between surfaces 601 may be setby the user), or crevasse splays or levees (fluviatile or turbiditic).Each of these associated/related formations may have their own rulesregarding the meshing of these formations (for instance, in FIG. 6c ,the size/shape/meshing of the cells in point bar zones 602 may bedifferent than the size/shape/meshing in the levee zone 603).

Thanks to this method, it is possible to adequately mesh the modelaccording to the needs and to the specific shape of the formations. If ameshing was performed prior to any formation determination, it isapparent that this meshing cannot fit the need of the modeling.

In addition, the shape of other geological formations may be determinedbased on a distance to a previously determined formation or/and to aprobability of existence of a surface of said other geologicalformations (function, for instance, of a distance (e.g. radial orlateral) to previously determined formations).

It is also possible to associate a facies (step 104 of FIG. 1) to eachcell of the newly created mesh (i.e. for each geological formation) asshown in FIG. 7 a.

This association may be based on:

-   -   quality index distributions QI_(i)(p) for each driver i function        of the considered (absolute or relative) position p (elements        703 and 704 being respectively the facies quality index        distribution function of the distance to the vertical axis        201-306 of the shape of the bed and the facies quality index        distribution function of the distance to the base 306 of the        bed),    -   facies proportions (column 701);    -   or on facies quality index ordering (column 702).

In this example of FIG. 7a , the quality index distributions arefunction of the distance to the vertical axis 201-306 of the shape ofthe bed and of the distance to the base 306 of the bed, but othergeological formations may have quality index distributions function ofother parameters set by the operator (i.e. the person setting themodeling).

For each cell of the geological formation that is considered, said cellhaving a position p, a cell quality index QI_(cell) is computed as beingQI_(cell)=Σ_(i)QI_(i)(p)/N (i being the current driver, N being thetotal number of drivers).

Then, the following process (see 705) may be used for associating afacies to a cell in a formation (having a plurality of cells):

-   -   /a/ selecting a cell with the lowest QI_(cell) within the cells        in the plurality of cells having no facies associated to;    -   /b/ associating, to said cell, the facies with the lowest        Quality index ordering (column 702) within the facies for which        the proportion is not reached (column 701)    -   /c/ reiterating step /a/ to /c/ until all cells in the plurality        of cells are associated with a facies.

It is apparent that the “lowest” words may be replaced by the “biggest”in said process.

It is also possible to associate a geological property (e.g.permeability, porosity, etc.)

(step 104 of FIG. 1) to each cell of the newly created mesh (i.e. foreach geological formation) as shown in FIG. 7 b.

This association may be based on property quality index distributionsQI_(i)(p) for each driver i function of the considered (absolute orrelative) position p (elements 713 and 714 being respectively theproperty quality index distribution function of the distance to thevertical axis 201-306 of the shape of the bed and the property qualityindex distribution function of the distance to the base 306 of the bed)and on property distribution (curve 711).

In this example of FIG. 7b , the property quality index distributionsare function of the distance to the vertical axis 201-306 of the shapeof the bed and of the distance to the base 306 of the bed, but othergeological formations may have property quality index distributionsfunction of other parameters set by the operator (i.e. the personsetting the modeling).

For each cell of the geological formation that is considered, said cellhaving a position p, a cell quality index QI_(cell) is computed as beingQI_(cell)=Σ_(i)QI_(i)(p)/N being the current driver, N being the totalnumber of drivers).

Then, the following process (see 715) may be used for associating aproperty to a cell in a formation (having a plurality of cells):

-   -   /a/ determining M random draw of property values in the property        distribution 711 (M being the number of cells in the plurality        of cells) and ordering said M random draw from the lowest to the        greatest value (see 712) (the index/rank/order of the random        draw for this ordering is the “property ordering));    -   /b/ selecting a cell with the lowest QI_(cell) within the cells        in the plurality of cells having no property associated to;    -   /c/ associating, to said cell, the random draw (property) with        the lowest property ordering (column 716) within the random        draws that have not been associated yet with a cell (column 712)    -   /d/ reiterating steps /a/ to /d/ until all cells in the        plurality of cells are associated with a property.

It is apparent that the “lowest” (respectively “biggest”) words may bereplaced by the “biggest” (respectively “lowest”) in said process.

For part(s) of the model that is/are not determined geologicalformations (i.e. background zone), it is possible to mesh (step 105 ofFIG. 1) it/them with common method(s) and to associate its/their cellswith property/facies (step 106 of FIG. 1) according to the relativeposition of the cells in regard of the geological formation determined(e.g. facies probabilities may be set by the operator according to aradial/lateral distance of a determined geological formation).

FIG. 8 is a possible embodiment for dynamically determining flow speedfield in the model/in the zone (the “flow speed field” may representsthe speed of a particle or water in said field).

Indeed, it is apparent that the determination of the fluvial trajectoryor the determination of any trajectory in the model may be based on theflow speed or on the gradient of the flow speed.

Then, it may be advantageous to ease the determination of a realisticflow speed field in the model.

The model (which could be a parametric model (u, v, t)) comprises atleast one stratigraphic layer (i.e. for a given t). In therepresentation of FIG. 8, only one stratigraphic layer is shown. A shoreline 800 splits the stratigraphic layer into two zones.

In continental zones (801) of the model, the flow speed (811) may bedetermined based on geological constraints (e.g. valleys, mountains,etc.). Nevertheless, in marine zones (802), said considerations are notrelevant. On the contrary, the flow speed (812) may be influenced bymarine streams.

Therefore, it is possible to define a transitional zone (i.e. betweenlines 800 and 822—marine transitional zone—and between lines 800 and821—continental transitional zone) where the flow speed field will havea transition between flow speed (811) in continental zone and flow speed(812) of the sea in the marine zone.

It is noted that the transition may be different in the marinetransitional zone and in the continental transitional zone.

For instance, in the continental transitional zone, the flow speed fieldmay be deformed so that the flow speed is perpendicular to the line 800,i.e. the limit between the continental zone 801 and the marine zone 802.In other words, the gradient of the flow speed is aligned with the shoreline 800.

For instance, in the marine transitional zone, the global flow speed 830field may be modified so that the flow speed at a given position is acombination of the flow speed at said given position if it was in acontinental zone (i.e. without the presence of sea) and the flow speed(812) of the sea at said position. Said combination may be weighted bythe distance of said position to the line 800. The weight used for saidcombination may be a linear weight or any other weight to smooth thetransition.

The combination of the flow speed at said given position may be afunction of the distance between said position and the line 800.

The combination of the flow speed at said given position may beS=αSc+(1−α)Sm where Sc is a vector representing the speed flow (811) inthe continental zone (i.e. above line 800), Sm is a vector representingthe flow speed (812) of the sea (i.e. below line 800)), S is a vectorrepresenting the global flow speed (830) and a is a number between 0and 1. α may be a function of the position and of the distance to theline 800. For instance, α may be 1 when the position is in thecontinental zone (i.e. above line 800) or when the position is aboveline 821 (i.e. in the continental zone but not in the continentaltransitional zone). Another option is to set the transitional zone as avoid zone (i.e. line 821 and line 800 being the same line). α may belinear, exponential or logarithmic in the marine zone or in the marinetransitional zone. For instance, in the marine transitional zone, α maybe a sigmoid or a logistic function (S shape).

The size of the continental transitional zone and the size of the marinetransitional zone is not necessarily the same.

It is also important to note that the model may be a parametric modelM_(p)(u,v,t) and thus may depend of the time. Therefore, the line 800(separating the continental zone and the marine zone) may change betweentwo times t1 and t2.

Therefore, it is possible to recompute the flow speed field at eachincrement of t (if, for instance, line 800 has changed in between saidincrement). Interpolation may be performed between two increments.

In addition, the flow speed 812 of the sea may be determined based onhydrodynamic modeling.

FIG. 9a is a possible embodiment for creating point bar zones such asdescribed in FIG. 6a, 6b or 6 c. A point bar is a depositional featuremade of alluvium that accumulates on the inside bend of streams andrivers below the slip-off slope. Point bars are found in abundance inmature or meandering streams. They are crescent-shaped and located onthe inside of a stream bend, being very similar to, though often smallerthan, towheads, or river islands.

To create in the model said point bar zones, it is proposed to firstcreate a fluvial geological formation such as described in FIG. 2a or 2b (lines 901 and 903 are the external bed of the fluvial geologicalformation—line 902 may be similar to trajectory 201 in FIG. 2b ). It isnoted that the representation of FIG. 9a is a 2D representation, but theformation and the modeling may be 3D using for instance B-splines,NURBS, etc. (i.e. parametric surfaces).

In order to define line 902, it is possible to parametrize a stochasticsimulation based on seismic images where the external geologicalformation may be visible. As a matter of fact, line 902 may also bedetermined directly based on the seismic image without any stochasticsimulation of the trajectory.

Once said fluvial geological formation is determined, it is possible toidentify points (911, 912, 913) of lines 902 where there is aninflection (i.e. inflection points). Any methods to determine inflectionpoints or approximation of real inflection points may be used todetermine said points. In the following, the wording “inflection points”are used even if the determined points are not all the inflection points(i.e. a subset of inflection points having specific characteristics) oreven if said points are only approximations of inflection points.

Once said “inflection points” are determined, it is possible to slightlydeform line 902 to reduce the curvature of the line 902. Saiddeformation of line 902 will define a new line 922. Said line 922 alsogoes through inflection points.

Once said line 922 is defined, the new surface (lines 921 and 923) of afluvial geological formation may be defined as previously described.

As described in relation with FIGS. 3b and 3c , it is possible torecompute parametric surfaces (e.g. NURBS) to subtract the previousfluvial geological formation defined by lines 901 and 903 to the currentfluvial geological formation defined by lines 921 and 923.

It is apparent that it is possible to reiterate the deformation of line902 or 922 and the subtraction of the newly defined fluvial geologicalformation with the former defined fluvial geological formations.

The reiteration may be limited by a predetermined number of iterations,by a percentage of deformation, by geometrical constraints of theformation or a combination of the latter.

In addition, it is possible to associate with each fluvial geologicalformation (that are the point bars) geological properties such astransmissivity limitation.

It is noted that said method may be used to determine point bars for asame stratigraphic layer (i.e. for a given stratigraphic time).

FIG. 9b is a possible embodiment for determining fluvial formations fordifferent stratigraphic layers.

The model 951 is a 2D model for the sake of the representation but a 3Dmodel with different stratigraphic layers is possible.

In said model 952, “no-flow” zones 952 and 953 (i.e. zones where fluvialformations cannot exists) may be defined.

As described previously, a fluvial formation 954 (with or without pointbar) may be determined (e.g. manually or via a stochastic process). Oncesaid fluvial formation 954 is determined, it is possible to define azone (955) around said fluvial formation to add constraints fordetermination of future fluvial formations. The limits of the zone 955(named constraint zone) may be at a predetermined distance of thefluvial formation 954. The distance may be any mathematical distancesuch as a Manhattan distance or a Euclidian distance.

Once said constraint zone is defined, it is possible to reiterate astochastic determination of a new fluvial formation with the constraintsthat every point of said new fluvial formation is within said constraintzone: for instance, if a point of the new determined fluvial zone isoutside said constraint zone, it is possible to reiterate thedetermination of said point as long as the point is not in theconstraint zone (if the number of reiteration for said point exceeds apredetermined number, it is possible to reinitialize the stochasticdetermination of the whole fluvial formation or to keep said point evenif it is not in the constraint zone). If a point of the new determinedfluvial zone is outside said constraint zone, it is also possible tomove said point to the nearest point of the constraint zone and thus tocontinue with said point for the stochastic determination. It is alsopossible to first try to reiterate the determination of said point aslong as the point is not in the constraint zone and if the number ofreiteration for said point exceeds a predetermined number, it ispossible to move said point as stated above.

A plurality of new fluvial formations may be determined with theconstraint zone 955. Alternatively, a new constraint zone is determinedfor each new fluvial formation and said new constraint zone is used forthe next determination of the fluvial formation. It is also possible touse the first determined constraint zone but to add a displacement(horizontal and/or vertical) that may be a function of the stratigraphiclayer (i.e. the geological time) used for the determination of a fluvialformation.

FIG. 10 is a representation of the modeling of bars (i.e. at an end ofthe fluvial formation) in marine zones of the model, especially in caseof tide-dominated deltas.

The shape of a delta is influenced by sediment input, wave energy, andtidal energy. Deltas which undergo strong tidal interaction areclassified as tide-dominated deltas. As sediment travels out of thedelta into the sea, high tides and flood tides confine sediment on thedelta plain and low tides carry sediment seaward. Tide-dominated deltastypically occur in locations of large tidal ranges or high tidal currentspeeds.

For instance, the model may comprise a continental zone 1002, a marinezone 1001 delimited by a shore line 1000. In said model, a fluvialformation 1003 has been determined.

When it is determined that the model comprises a tide-dominated delta(manually or via determination of the speed flow of the sea and of thecontinental zone and comparison with the flow speed in the fluvialformation), it is possible to define a delta zone (for instance atriangular zone, a circular sector, etc.).

The shape of the delta zone (for instance in the furthest part of thedelta zone, in regard of the fluvial formation, i.e. line 1005) may be afunction of the marine flow speed and the flow speed in the fluvialformation.

In addition, the delta zone may be parametrized by the delta angle θ,the thickness of the deposit for the lobes, the distance d₁ or d₂(depending of the form of the delta). For instance, if the flow speed inthe fluvial formation is important, the distance may increase.

In order to determine the location of the tidal bars in the delta zonethat has been defined (for each stratigraphic layer, for instance), itis possible to determine stochastic trajectories from point 1006 (i.e.the end of the fluvial formation 1003 and the beginning of the deltazone) taking into account (optionally) the fluvial flow speed and/or themarine flow speed. The determined trajectories are determined inside thedelta zone 1004. The determination of the trajectory ends when a pointof the trajectory is determined outside the delta zone.

During the determination of the trajectory, it is possible tostochastically determine if the new point that is being determined forthe trajectory is a location for a bar. Alternatively, it is possible todetermine the full trajectory and then determine points of saidtrajectory where a bar is located.

Therefore, it is possible to insert in the model bars at the determinedlocations.

The form and thickness of the bars may depend on the marine flow speedat the location of the bars. Therefore, a database where acorrespondence between range of flow speed and forms of bars may havebeen predetermined.

FIG. 11 is a representation of the modeling of the flow speed (or thegradient of the flow speed) in the model for a stratigraphic layer.

In the prior art, a plurality of methods has been developed to determinethe flow speed field in the model. For instance, in a former method,objects in the model should be identified (e.g. architectural elements)and for each object a privileged direction of flow should be indicated.Nevertheless, said identification may be long, difficult and subjective.

In said proposed method, proportion cubes are used. Indeed, proportioncubes are often already available in geological modeling (determinedthanks to seismic images, well data, etc.).

A facies proportion cube is a description of the reservoir model interms of vectorial properties (each cell of the cube contains theprobability of occurrence of each facies represented in the model). Thecube is then a representation of the distribution of facies and may beassociated with uncertainties. The cube may be a function of theposition (u,v,t) in the model or a plurality of cubes may be defined,one for each defined zone of the model.

In the present method, it is first possible to define no-flow zones(i.e. the mountain-shape zones in the example of map 1101) (optional).

Based on the available proportion cubes, it is possible to determine foreach location (or for a plurality of locations) of the model arespective property value, for example a permeability value (each shadeof grey represents a respective pseudo-permeability value in map 1102).Indeed, as the proportion cube contains the probability of occurrence ofeach facies and as each facies as a given permeability, the local(pseudo) permeability may be easily determined.

If proportion cubes are not available for some points/locations of themodel, it is possible to compute a local mean (with a given window/witha given distance around said points) to create information associated topseudo-permeability to said points. It is possible to use aninterpolation algorithm.

The permeability value may be set to zero for no-flow zones.

Once the permeability map is determined (map 1102), it is possible todetermine the gradient of the flow speed based on said permeability map.Indeed, by solving the Darcy-Weisbach equation (with a given hydraulicload), it is possible to obtain a gradient flow speed field (element1103, where a line with a same shade of grey represents an iso-valueline of the gradient field—the trajectories could be perpendicular tosaid iso-value lines).

Therefore, the (for instance, stochastic) trajectory may be determinedthanks to said gradient flow speed as explained before, based on theproportion cubes. Therefore, there is no need of any azimuth map.

FIG. 12 is a possible embodiment for a device that enables the presentdisclosure.

In this embodiment, the device 1200 comprises a computer, this computercomprising a memory 1205 to store program instructions loadable into acircuit and adapted to cause circuit 1204 to carry out the steps of thepresent disclosure when the program instructions are run by the circuit1204.

The memory 1205 may also store data and useful information for carryingthe steps of the present disclosure as described above.

The circuit 1204 may be for instance:

-   -   a processor or a processing unit adapted to interpret        instructions in a computer language, the processor or the        processing unit may comprise, may be associated with or be        attached to a memory comprising the instructions, or    -   the association of a processor/processing unit and a memory, the        processor or the processing unit adapted to interpret        instructions in a computer language, the memory comprising said        instructions, or    -   an electronic card wherein the steps of the disclosure are        described within silicon, or    -   a programmable electronic chip such as a FPGA chip (for        «Field-Programmable Gate Array»).

This computer comprises an input interface 1203 for the reception ofdata/model/input used for the above method according to the disclosureand an output interface 1206 for providing a complete model to anexternal device 1207.

To ease the interaction with the computer, a screen 1201 and a keyboard1202 may be provided and connected to the computer circuit 1204.

Expressions such as “comprise”, “include”, “incorporate”, “contain”,“is” and “have” are to be construed in a non-exclusive manner wheninterpreting the description and its associated claims, namely construedto allow for other items or components which are not explicitly definedalso to be present. Reference to the singular is also to be construed inbe a reference to the plural and vice versa.

A person skilled in the art will readily appreciate that variousparameters disclosed in the description may be modified and that variousembodiments disclosed may be combined without departing from the scopeof the disclosure. These and other changes can be made to theembodiments in light of the above-detailed description. In general, inthe following claims, the terms used should not be construed to limitthe claims to the specific embodiments disclosed in the specificationand the claims, but should be construed to include all possibleembodiments along with the full scope of equivalents to which suchclaims are entitled. Accordingly, the claims are not limited by thedisclosure.

1. A method for determination of a real subsoil geological formation,comprising: receiving a model representing the real subsoil, said modelcomprising a stratigraphic layer, said stratigraphic layer comprising ashore line dividing the stratigraphic layer into a continental zone anda marine zone; receiving a first flow speed field representative of acontinental domain for the stratigraphic layer; receiving a second flowspeed field representative of a marine domain for the stratigraphiclayer; determining a global flow speed field, the global flow speedfield including a weighted combination of the first flow speed field andthe second flow speed field for each position in the stratigraphiclayer, weights of the combination being based on a distance of saidposition to the shore line and whether the position is within thecontinental zone or the marine zone; and determining a real subsoilgeological formation for the stratigraphic layer based on the determinedglobal flow speed field.
 2. The method of claim 1, wherein the receivedsecond flow speed field or the received first flow speed field isdetermined based on hydrodynamic modeling.
 3. The method of claim 1,wherein the received second flow speed field or the received first flowspeed field is determined based on the shore line.
 4. The method ofclaim 1, wherein, before the determining the global flow speed field,the first flow speed is modified to align a gradient of the first flowspeed field with the shore line.
 5. The method of claim 1, wherein themodel comprises a plurality of stratigraphic layers, each stratigraphiclayer within said plurality comprises a respective shore line dividingthe stratigraphic layer into a respective continental zone and arespective marine zone, wherein the receiving the first flow speed, thereceiving the second flow speed, the determining the global flow speedfield, and the determining the real subsoil geological formation arereiterated for each stratigraphic layer within said plurality.
 6. Themethod of claim 5, wherein the respective shore line for eachstratigraphic layer within said plurality is different from therespective shore line for the other stratigraphic layer within saidplurality.
 7. The method of claim 1, wherein an intersection between atransitional zone and the continental zone is void or is the shore line.8. A device for determination of a real subsoil geological formation,comprising: an interface configured to receive a model representing thereal subsoil, said model comprising a stratigraphic layer, saidstratigraphic layer comprising a shore line dividing the stratigraphiclayer into a continental zone and a marine zone (802); an interfaceconfigured to receive a first flow speed field for the stratigraphiclayer representative of a continental domain; an interface configured toreceive a second flow speed field representative of a marine domain forthe stratigraphic layer; a circuit configured to determine a global flowspeed field, the global flow speed field including a weightedcombination of the first flow speed field and the second flow speedfield for each position in the stratigraphic layer, weights of thecombination being based on a distance of said position to the shore lineand whether the position is within the continental zone or the marinezone; and a circuit configured to determine the real subsoil compositionfor the stratigraphic layer based on the determined global flow speedfield.
 9. A non-transitory computer readable storage medium, havingstored thereon a computer program comprising program instructions, thecomputer program being loadable into a data-processing device andadapted to cause the data-processing device to perform a method fordetermination of a real subsoil geological formation when the computerprogram is run by the data-processing device, the method comprising:receiving a model representing the real subsoil, said model comprising astratigraphic layer, said stratigraphic layer comprising a shore linedividing the stratigraphic layer into a continental zone and a marinezone (802); receiving a first flow speed field representative of acontinental domain for the stratigraphic layer; receiving a second flowspeed field representative of a marine domain for the stratigraphiclayer; determining a global flow speed field, the global flow speedfield including a weighted combination of the first flow speed field andthe second flow speed field for each position in the stratigraphiclayer, weights of the combination being based on a distance of saidposition to the shore line and whether the position is within thecontinental zone or the marine zone; and determining a real subsoilgeological formation for the stratigraphic layer based on the determinedglobal flow speed field.
 10. The non-transitory computer readablestorage medium of claim 9, wherein the received second flow speed fieldor the received first flow speed field is determined based onhydrodynamic modeling.
 11. The non-transitory computer readable storagemedium of claim 9, wherein the received second flow speed field or thereceived first flow speed field is determined based on the shore line.12. The non-transitory computer readable storage medium of claim 9,wherein, before the determining the global flow speed field, the firstflow speed is modified to align a gradient of the first flow speed fieldwith the shore line.
 13. The non-transitory computer readable storagemedium of claim 9, wherein the model comprises a plurality ofstratigraphic layers, each stratigraphic layer within said pluralitycomprises a respective shore line dividing the stratigraphic layer intoa respective continental zone and a respective marine zone, wherein thereceiving the first flow speed, the receiving the second flow speed, thedetermining the global flow speed field, and the determining the realsubsoil geological formation are reiterated for each stratigraphic layerwithin said plurality.
 14. The non-transitory computer readable storagemedium of claim 13, wherein the respective shore line for eachstratigraphic layer within said plurality is different from therespective shore line for the other stratigraphic layer within saidplurality.
 15. The non-transitory computer readable storage medium ofclaim 9, wherein an intersection between a transitional zone and thecontinental zone is void or is the shore line.